
sedimentary
Chert (Jasper/Flint variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Brown, tan, and reddish-orange due to iron oxides. Luster: Dull to waxy. Crystal structure: Cryptocrystalline (microscopic quartz crystals). Cleavage: None, exhibits conchoidal (shell-like) fracture.
- Hardness
- 7 on Mohs scale
- Color
- Brown, tan, and reddish-orange due to iron oxides
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Brown, tan, and reddish-orange due to iron oxides. Luster: Dull to waxy. Crystal structure: Cryptocrystalline (microscopic quartz crystals). Cleavage: None, exhibits conchoidal (shell-like) fracture.
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like diatoms or radiolaria) or through chemical precipitation in sedimentary environments. Often found as nodules in limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers) due to its sharp edges. Modernly used in road construction as aggregate and occasionally as semi-precious gemstones for jewelry (Jasper/Agate).
Geological facts
Chert was one of the most important minerals for early humans because of its ability to be knapped into sharp tools. It is also used as a fire-starter when struck against steel to create sparks.
Field identification & locations
Identify in the field by its hardness (it will scratch glass and steel) and its smooth, curved conchoidal fractures. Commonly found in riverbeds, glacial till, and limestone outcrops globally.
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